Official Series Description


Lab Data Summary

Aggregate lab data for the SCANTIC soil series. This aggregation is based on all pedons with a current taxon name of SCANTIC, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to SCANTIC were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
14210N0725S09VT007003Scantic6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4444656,-73.0970993
14210N0726S09VT007004Scantic6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4444656,-73.0970993
14340A3949S1976VT015007Scantic7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5544434,-72.6144409
144A40A4075S1964NH017002SCANTIC5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1711121,-70.9330521
144B40A1277S1962ME005006Scantic6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6127396,-70.399704
144B40A1281S1976ME009001Scantic6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.432724,-68.3715744
144B96P0009S1995VT005003Scantic7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2233955,-72.0639818
144B96P0010S1995VT005003AScantic4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2161734,-72.0637039

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SCANTIC soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SCANTIC series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the SCANTIC series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the SCANTIC series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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Competing Series

Soil series competing with SCANTIC share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the SCANTIC series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the SCANTIC series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with SCANTIC, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MA-2012-02-02-05 | Essex County, Northern Part - February 1981

    Typical pattern of soils and parent material in the Scantic-Maybid-Buxton association (Soil Survey of Essex County, Massachusetts, Northern Part; February 1981).

  2. ME-2012-02-03-02 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Buxton-Scantic-Lyman map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  3. ME-2012-02-03-05 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Lyman-Peru-Scantic map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  4. ME-2012-02-03-16 | York County - June 1982

    Typical pattern of soils and underlying material in the Scantic-Raynham-Buxton association (Soil Survey of York County, Maine; June 1982).

  5. NH-2012-02-14-25 | Strafford County - March 1973

    Typical pattern of soils and underlying material in the Hollis-Charlton-Buxton-Scantic association (Soil Survey of Strafford County, New Hampshire; March 1973).

Map Units

Map units containing SCANTIC as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Scantic silt loam, 0 to 3 percent slopes16A2986790673vjrlma60519771:15840
Scantic silt loam, 3 to 8 percent slopes16B301790676vjrpma60519771:15840
Scantic silt loam, 0 to 3 percent slopesSn334543157332slv3me00519691:24000
Scantic silt loam, 0 to 3 percent slopesScA406972844972slv3me01119741:20000
Scantic silt loam, 0 to 3 percent slopesSc324372846592slv3me03119781:20000
Urban land-Scantic complex, 0 to 3 percent slopesUsA4552846719k6yme03119781:20000
Scantic silt loam, 0 to 3 percent slopesSc229472847342slv3me60119831:20000
Scantic silt loam, 0 to 3 percent slopesSc302452847922slv3me60219671:20000
Scantic silt loam, 0 to 3 percent slopesScA264732848712slv3me60619661:15840
Lamoine-Scantic-Buxton complex, 0 to 15 percent slopesLCB241722851092x1bqme61119881:20000
Scantic-Lamoine-Peru complex, 0 to 8 percent slopes, very stonySEB204562851382x1bxme61119881:20000
Scantic silt loam, 0 to 3 percent slopesSa191162851412slv3me61119881:20000
Scantic-Biddeford complex, 0 to 3 percent slopesSB136632851372t0jmme61119881:20000
Scantic-Lamoine complex, 0 to 8 percent slopes, very stonySdB92442851422x1bpme61119881:20000
Lamoine-Scantic complex, 0 to 8 percent slopesLbB52322851142x1bnme61119881:20000
Scantic-Biddeford complex, 0 to 3 percent slopesSBA51136742169sx8yme61220161:24000
Scantic-Lamoine-Colonel association, 0 to 8 percent slopes, very stonySLB15936742170sx8zme61220161:24000
Lamoine-Scantic complex, 0 to 8 percent slopesLAB7390742159sx8mme61220161:24000
Lamoine-Scantic complex, 0 to 8 percent slopesLsB6199741610swpxme61220161:24000
Scantic silt loam, 0 to 3 percent slopesScA2841741913sx0pme61220161:24000
Biddeford-Scantic-Lamoine complex, 0 to 8 percent slopes, very stonyBxB244422851832x1c5me61419601:20000
Scantic silt loam, 0 to 8 percent slopesScB82022852642x1c0me61419601:20000
Lamoine-Buxton-Scantic complex, 0 to 15 percent slopesLCB988322855822t0kbme61720041:24000
Scantic-Biddeford complex, 0 to 3 percent slopesSF570682856142t0jmme61720041:24000
Lamoine-Scantic-Colonel complex, 0 to 8 percent slopes, very stonyLSB240162855852x1brme61720041:24000
Lamoine-Tunbridge-Scantic complex, 0 to 8 percent slopes, very stonyLTB226452855862x1btme61720041:24000
Lamoine-Rawsonville-Scantic complex, 0 to 8 percent slopes, very stonyLKB2004414012671j145me61720041:24000
Lamoine-Scantic complex, 0 to 8 percent slopesLmB65802855912x1bnme61720041:24000
Scantic silt loam, 0 to 3 percent slopesSa27792856202slv3me61720041:24000
Lamoine-Creasey-Scantic complex, 0 to 8 percent slopesLEB27022855839l5cme61720041:24000
Scantic-Lamoine complex, 0 to 8 percent slopes, very stonyLnB7782855922x1bpme61720041:24000
Scantic-Biddeford complex, 0 to 3 percent slopesSBA452219090852t0jmme62220071:24000
Lamoine-Buxton-Scantic complex, 0 to 15 percent slopesLBC316119090842t0kbme62220071:24000
Lamoine-Scantic-Colonel complex, 0 to 8 percent slopes, very stonyLLB194419090832x1brme62220071:24000
Lamoine-Tunbridge-Scantic complex, 0 to 8 percent slopes, very stonyLNB104719090822x1btme62220071:24000
Scantic-Lamoine-Peru complex, 0 to 8 percent slopes, very stonySLB103419092802x1bxme62220071:24000
Lamoine-Scantic-Buxton complex, 0 to 15 percent slopesLEB38019092242x1bqme62220071:24000
Scantic silt loam, 0 to 3 percent slopesScA69052799239d8snh01719681:20000
Scantic silt loam, 3 to 8 percent slopesScB9522799249d8tnh01719681:20000
Scantic silty clay loam, 0 to 3 percent slopesSdA70372677791bmntny04920181:24000
Scantic silt loam, 0 to 3 percent slopes47A2102829212slv3vt00520061:20000
Scantic silt loam, 0 to 2 percent slopesScA34962817499g5pvt00719691:15840
Scantic silt loam, 2 to 6 percent slopesScB21402817509g5qvt00719691:15840
Scantic silt loam, 0 to 3 percent slopesScA75832818489g8wvt01119761:20000
Scantic silt loam, 3 to 8 percent slopesScB8062818499g8xvt01119761:20000
Scantic variant bouldery silt loam, 8 to 25 percent slopesSeD3162819439gcyvt01519791:20000
Scantic variant bouldery silt loam, 25 to 50 percent slopesSeE2092819449gczvt01519791:20000
Scantic silt loam, 0 to 3 percent slopes50A15372834852slv3vt01920051:20000
Scantic silt loam, 0 to 3 percent slopes45A7562826722slv3vt02319961:20000

Map of Series Extent

Approximate geographic distribution of the SCANTIC soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .